11 years of Rayleigh Lidar Observations of Gravity Wave Activity above the Southern Tip of South America

International audience Gravity wave (GW) activity is analyzed using temperature (T) data retrieved from a Rayleigh lidar at Río Gallegos, Argentina (51.6°S, 69.3°W). GW characteristics are derived from 302 nights of observations providing more than 1018 h of high‐resolution lidar data between 20 km...

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Published in:Journal of Geophysical Research: Atmospheres
Main Authors: Llamedo, P., Salvador, J., de La Torre, A., Quiroga, J., Alexander, P., Hierro, R., Schmidt, T., Pazmino, Andrea, Quel, E.
Other Authors: Laboratorio de Investigación, Desarrollo y Transferencia de la Universidad Austral (LIDTUA), Consejo Nacional de Investigaciones Científicas y Técnicas Buenos Aires (CONICET)-Universidad Austral, Centro de Investigaciones en Láseres y Aplicaciones Buenos Aires (CEILAP), Consejo Nacional de Investigaciones Científicas y Técnicas Buenos Aires (CONICET)-Instituto de Investigaciones Científicas y Técnicas para la Defensa (CITEDEF), Facultad Regional Buenos Aires (UTN-FRBA), Universidad Tecnológica Nacional Sarmiento (UTN), Universidad Nacional de la Patagonia Austral (UNPA), Instituto de Física de Buenos Aires (IFIBA), Consejo Nacional de Investigaciones Científicas y Técnicas Buenos Aires (CONICET)-Facultad de Ciencias Exactas y Naturales Buenos Aires (FCEyN), Universidad de Buenos Aires Buenos Aires (UBA)-Universidad de Buenos Aires Buenos Aires (UBA), German Research Centre for Geosciences - Helmholtz-Centre Potsdam (GFZ), STRATO - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2019
Subjects:
Online Access:https://insu.hal.science/insu-01960146
https://insu.hal.science/insu-01960146/document
https://insu.hal.science/insu-01960146/file/2018JD028673.pdf
https://doi.org/10.1029/2018JD028673
id ftinsu:oai:HAL:insu-01960146v1
record_format openpolar
institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language English
topic [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
spellingShingle [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
Llamedo, P.
Salvador, J.
de La Torre, A.
Quiroga, J.
Alexander, P.
Hierro, R.
Schmidt, T.
Pazmino, Andrea
Quel, E.
11 years of Rayleigh Lidar Observations of Gravity Wave Activity above the Southern Tip of South America
topic_facet [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
description International audience Gravity wave (GW) activity is analyzed using temperature (T) data retrieved from a Rayleigh lidar at Río Gallegos, Argentina (51.6°S, 69.3°W). GW characteristics are derived from 302 nights of observations providing more than 1018 h of high‐resolution lidar data between 20 km and 56 km height from August 2005 to December 2015. T measurements are performed by a Differential Absorption lidar (DIAL) instrument. This lidar was the southernmost outside Antarctica until the end of 2017. Río Gallegos is an exceptional place to observe large amplitude GW. Every lidar measurement is classified according to its relative position to the polar vortex. The lidar measurements are compared with collocated Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) and Global Positioning System‐Radio Occultation (GPS‐RO) data. The different instruments show different windows of the GW spectrum, providing complementary observations. In general, the geometric mean of the specific GW potential energy (PE) is larger during winter and spring than during summer and autumn. The largest geometric mean of PE is found inside the vortex and decreases monotonically at its edge, outside it and when there is no vortex. The same behavior is observed with satellite data. On average, it can be seen that lidar observations provide larger PE values than limb sounding measurements. From a Morlet continuous wavelet transform analysis, 3 distinct modes are captured from SABER and from GPS RO data at the upper and lower stratosphere, respectively. In particular, a systematic 3.5‐4 years oscillation, possibly related to El Niño–Southern Oscillation is observed.
author2 Laboratorio de Investigación, Desarrollo y Transferencia de la Universidad Austral (LIDTUA)
Consejo Nacional de Investigaciones Científicas y Técnicas Buenos Aires (CONICET)-Universidad Austral
Centro de Investigaciones en Láseres y Aplicaciones Buenos Aires (CEILAP)
Consejo Nacional de Investigaciones Científicas y Técnicas Buenos Aires (CONICET)-Instituto de Investigaciones Científicas y Técnicas para la Defensa (CITEDEF)
Facultad Regional Buenos Aires (UTN-FRBA)
Universidad Tecnológica Nacional Sarmiento (UTN)
Universidad Nacional de la Patagonia Austral (UNPA)
Instituto de Física de Buenos Aires (IFIBA)
Consejo Nacional de Investigaciones Científicas y Técnicas Buenos Aires (CONICET)-Facultad de Ciencias Exactas y Naturales Buenos Aires (FCEyN)
Universidad de Buenos Aires Buenos Aires (UBA)-Universidad de Buenos Aires Buenos Aires (UBA)
German Research Centre for Geosciences - Helmholtz-Centre Potsdam (GFZ)
STRATO - LATMOS
Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Llamedo, P.
Salvador, J.
de La Torre, A.
Quiroga, J.
Alexander, P.
Hierro, R.
Schmidt, T.
Pazmino, Andrea
Quel, E.
author_facet Llamedo, P.
Salvador, J.
de La Torre, A.
Quiroga, J.
Alexander, P.
Hierro, R.
Schmidt, T.
Pazmino, Andrea
Quel, E.
author_sort Llamedo, P.
title 11 years of Rayleigh Lidar Observations of Gravity Wave Activity above the Southern Tip of South America
title_short 11 years of Rayleigh Lidar Observations of Gravity Wave Activity above the Southern Tip of South America
title_full 11 years of Rayleigh Lidar Observations of Gravity Wave Activity above the Southern Tip of South America
title_fullStr 11 years of Rayleigh Lidar Observations of Gravity Wave Activity above the Southern Tip of South America
title_full_unstemmed 11 years of Rayleigh Lidar Observations of Gravity Wave Activity above the Southern Tip of South America
title_sort 11 years of rayleigh lidar observations of gravity wave activity above the southern tip of south america
publisher HAL CCSD
publishDate 2019
url https://insu.hal.science/insu-01960146
https://insu.hal.science/insu-01960146/document
https://insu.hal.science/insu-01960146/file/2018JD028673.pdf
https://doi.org/10.1029/2018JD028673
long_lat ENVELOPE(-67.150,-67.150,-68.133,-68.133)
geographic Argentina
Gallegos
geographic_facet Argentina
Gallegos
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source ISSN: 2169-897X
EISSN: 2169-8996
Journal of Geophysical Research: Atmospheres
https://insu.hal.science/insu-01960146
Journal of Geophysical Research: Atmospheres, 2019, 124 (2), pp.451-467. ⟨10.1029/2018JD028673⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1029/2018JD028673
insu-01960146
https://insu.hal.science/insu-01960146
https://insu.hal.science/insu-01960146/document
https://insu.hal.science/insu-01960146/file/2018JD028673.pdf
doi:10.1029/2018JD028673
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1029/2018JD028673
container_title Journal of Geophysical Research: Atmospheres
container_volume 124
container_issue 2
container_start_page 451
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spelling ftinsu:oai:HAL:insu-01960146v1 2023-11-12T04:02:12+01:00 11 years of Rayleigh Lidar Observations of Gravity Wave Activity above the Southern Tip of South America Llamedo, P. Salvador, J. de La Torre, A. Quiroga, J. Alexander, P. Hierro, R. Schmidt, T. Pazmino, Andrea Quel, E. Laboratorio de Investigación, Desarrollo y Transferencia de la Universidad Austral (LIDTUA) Consejo Nacional de Investigaciones Científicas y Técnicas Buenos Aires (CONICET)-Universidad Austral Centro de Investigaciones en Láseres y Aplicaciones Buenos Aires (CEILAP) Consejo Nacional de Investigaciones Científicas y Técnicas Buenos Aires (CONICET)-Instituto de Investigaciones Científicas y Técnicas para la Defensa (CITEDEF) Facultad Regional Buenos Aires (UTN-FRBA) Universidad Tecnológica Nacional Sarmiento (UTN) Universidad Nacional de la Patagonia Austral (UNPA) Instituto de Física de Buenos Aires (IFIBA) Consejo Nacional de Investigaciones Científicas y Técnicas Buenos Aires (CONICET)-Facultad de Ciencias Exactas y Naturales Buenos Aires (FCEyN) Universidad de Buenos Aires Buenos Aires (UBA)-Universidad de Buenos Aires Buenos Aires (UBA) German Research Centre for Geosciences - Helmholtz-Centre Potsdam (GFZ) STRATO - LATMOS Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) 2019 https://insu.hal.science/insu-01960146 https://insu.hal.science/insu-01960146/document https://insu.hal.science/insu-01960146/file/2018JD028673.pdf https://doi.org/10.1029/2018JD028673 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2018JD028673 insu-01960146 https://insu.hal.science/insu-01960146 https://insu.hal.science/insu-01960146/document https://insu.hal.science/insu-01960146/file/2018JD028673.pdf doi:10.1029/2018JD028673 info:eu-repo/semantics/OpenAccess ISSN: 2169-897X EISSN: 2169-8996 Journal of Geophysical Research: Atmospheres https://insu.hal.science/insu-01960146 Journal of Geophysical Research: Atmospheres, 2019, 124 (2), pp.451-467. ⟨10.1029/2018JD028673⟩ [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] info:eu-repo/semantics/article Journal articles 2019 ftinsu https://doi.org/10.1029/2018JD028673 2023-11-01T17:25:49Z International audience Gravity wave (GW) activity is analyzed using temperature (T) data retrieved from a Rayleigh lidar at Río Gallegos, Argentina (51.6°S, 69.3°W). GW characteristics are derived from 302 nights of observations providing more than 1018 h of high‐resolution lidar data between 20 km and 56 km height from August 2005 to December 2015. T measurements are performed by a Differential Absorption lidar (DIAL) instrument. This lidar was the southernmost outside Antarctica until the end of 2017. Río Gallegos is an exceptional place to observe large amplitude GW. Every lidar measurement is classified according to its relative position to the polar vortex. The lidar measurements are compared with collocated Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) and Global Positioning System‐Radio Occultation (GPS‐RO) data. The different instruments show different windows of the GW spectrum, providing complementary observations. In general, the geometric mean of the specific GW potential energy (PE) is larger during winter and spring than during summer and autumn. The largest geometric mean of PE is found inside the vortex and decreases monotonically at its edge, outside it and when there is no vortex. The same behavior is observed with satellite data. On average, it can be seen that lidar observations provide larger PE values than limb sounding measurements. From a Morlet continuous wavelet transform analysis, 3 distinct modes are captured from SABER and from GPS RO data at the upper and lower stratosphere, respectively. In particular, a systematic 3.5‐4 years oscillation, possibly related to El Niño–Southern Oscillation is observed. Article in Journal/Newspaper Antarc* Antarctica Institut national des sciences de l'Univers: HAL-INSU Argentina Gallegos ENVELOPE(-67.150,-67.150,-68.133,-68.133) Journal of Geophysical Research: Atmospheres 124 2 451 467